BLOCKSTONE COLLECTION - Marshalls...Marshalls was founded in the 1890’s when Solomon Marshall...
Transcript of BLOCKSTONE COLLECTION - Marshalls...Marshalls was founded in the 1890’s when Solomon Marshall...
w w w . m a r s h a l l s . c o . u k / n a t u r a l s t o n e
B L O C K S T O N E C O L L E C T I O N
Marshalls wasfounded in the 1890’s
when Solomon Marshall first quarried and
produced Cromwell Yorkstone from the
hillside at Southowram.
Since then, Marshalls has developed into the country’s leading supplier of natural stone, as well as commercial hard landscaping products, linear drainage and street furniture.The experience gained from those early days has enabled Marshalls to evolve and adapt to meet customer needs, becoming the most innovative and exciting stone supplier in the country.
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Greenmoor
Doddington
Fletcher Bank
Howley Park
Lazonby
Locharbriggs
Moselden
Haslingden Bed
Stanton Moor
St Bee’s
Stoke Hall
Key:
Quarries
UK operations
landscaping features ashlar
steps street furniture
rainscreen cladding stone art
43
PHYSICAL PERFORMANCE OF GREENMOOR
GEOLOGICAL TYPEMillstone Grit Series, CarboniferousSandstone
PETROGRAPHIC DESCRIPTION Pale greenish grey fine grained sandstone BSEN 12407: 2000
APPARENT DENSITY 2432 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 10% BSEN 1936: 2006
FLEXURAL STRENGTH (PARALLEL) MEANFLEXURAL STRENGTH (PERPENDICULAR) MEAN
15.15 MPa9.9 MPa BSEN 13161: 2008
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
Greenmoor is a true Yorkstone, with a well established quarry near Huddersfield in West Yorkshire. Used all over the UK, Greenmoor is a brown to blue fine grained stone, with a beautiful aesthetic look and feel.
A Carboniferous sandstone from
Huddersfield, West Yorkshire. Greenmoor is
one of the most popular sandstones chosen for a wide variety of
projects nationwide.
Huddersfield, West Yorkshire
British Yorkstone GREENMOOR
British Yorkstone GREENMOOR
65
PHYSICAL PERFORMANCE OF DODDINGTON
GEOLOGICAL TYPEMillstone Grit Series, CarboniferousSandstone
PETROGRAPHIC DESCRIPTIONPink to pale pink/purple mainly fine grained sandstone
BSEN 12407: 2000
APPARENT DENSITY 2110 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 20.4% BSEN 1936: 2006
FLEXURAL STRENGTH (PARALLEL) MEANFLEXURAL STRENGTH (PERPENDICULAR) MEAN
3.3 MPa3.1 MPa BSEN 13161: 2008
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
Sporting a unique and consistent pink colouration and a mainly fine grained appearance. Doddington hails from Northumberland, with quarry records dating back until 1897 it is proven to be popular due to its colouring and durable characteristics and has extensive reserves available
A Carboniferous sandstone from the Doddington Quarry in Northumberland,
Doddington is a very durable sandstones
chosen for a wide variety of projects
nationwide.
Northumberland, UK
British Sandstone DODDINGTON
British Sandstone DODDINGTON
87
PHYSICAL PERFORMANCE OF FLETCHER BANK
GEOLOGICAL TYPEMillstone Grit Series, CarboniferousSandstone
PETROGRAPHIC DESCRIPTION
Pale grey to palebuff / buff, fine to medium to coarse grained sandstone
BSEN 12407: 2000
APPARENT DENSITY 2310 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 12.8% BSEN 1936: 2006
FLEXURAL STRENGTH (PARALLEL) MEANFLEXURAL STRENGTH (PERPENDICULAR) MEAN
4.4 MPa5.4 MPa BSEN 13161: 2008
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
Fletcher Bank is a millstone grit from the Carboniferous period hailing from a quarry near Ramsbottom, Lancashire. Buff to grey in colouration, Fletcher Bank has been used in all manner of projects across the UK.
A Carboniferous sandstone from the
Fletcher Bank Quarry near Ramsbottom,
that is a very durable sandstones chosen for a wide variety of
projects nationwide.
Ramsbottom, Lancashire
British Sandstone FLETCHER BANK
British Sandstone FLETCHER BANK
109
PHYSICAL PERFORMANCE OF HOWLEY PARK
GEOLOGICAL TYPEMillstone Grit Series, CarboniferousSandstone
PETROGRAPHIC DESCRIPTION Pale greenish grey fine grained sandstone BSEN 12407: 2000
APPARENT DENSITY 2432 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 10% BSEN 1936: 2006
FLEXURAL STRENGTH (PERPENDICULAR) MEAN 17 MPa BSEN 13161: 2008
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
Howley Park is a buff to brown sandstone with a slight tonal variation runningthroughout the stone. The stones warm tones make it ideal for a variety of projects.
A Carboniferous sandstone from the Howley Park Quarry
in Leeds, West Yorkshire. It is one
of the most popular sandstones chosen for a wide variety of
projects nationwide.
Leeds, West Yorkshire
British Sandstone HOWLEY PARK
British Sandstone HOWLEY PARK
1211
PHYSICAL PERFORMANCE OF LAZONBYGEOLOGICAL TYPE Permian Sandstone
PETROGRAPHIC DESCRIPTION New red sandstone of permian age BSEN 12407: 2000
APPARENT DENSITY 2360 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 11.3% BSEN 1936: 2006
FLEXURAL STRENGTH (PARALLEL) MEANFLEXURAL STRENGTH (PERPENDICULAR) MEAN
5.8 MPa6.3 MPa BSEN 12372: 2006
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
Lazonby is a medium grained sandstone with a consistent salmon red colour, enhanced by the sparkle of quartz grains. A Permian Triassic Era material, extracted near Penrith, quarry records date back to 1878.
A Permian sandstone from near the
Penrith Quarry in Cumbria, Lazonby
is a very durable sandstone chosen
for a wide variety of projects nationwide.
Cumbria, UK
British Sandstone LAZONBY
British Sandstone LAZONBY
1413
PHYSICAL PERFORMANCE OF LOCHARBIGGSGEOLOGICAL TYPE Permian Sandstone
PETROGRAPHIC DESCRIPTION
Dark red to dark orange/red when wet, medium to coarse grained sandstone
BSEN 12407: 2000
APPARENT DENSITY 2000 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 24.3% BSEN 1936: 2006
FLEXURAL STRENGTH (PARALLEL) MEANFLEXURAL STRENGTH (PERPENDICULAR) MEAN
3.9 MPa5 MPa BSEN 12372: 2006
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
Quarried since the 18th century, this red to pink medium grained sandstone is widely specified across Scotland and England. The impressive list of reference sites forLocharbriggs Red sandstone dates back to the 1700s and includes sites across Scotland and England as well as major land mark buildings in Manchester,Glasgow and Edinburgh.
A Permian sandstone from the Locharbriggs
Quarry in Dumfries, Scotland, Locharbriggs is one of the oldest and largest actively worked red sandstone quarries
in Scotland today.
Dumfries, Scotland
British Sandstone LOCHARBRIGGS
British Sandstone LOCHARBRIGGS
1615
PHYSICAL PERFORMANCE OF MOSELDEN
GEOLOGICAL TYPEMillstone Grit Series, CarboniferousSandstone
PETROGRAPHIC DESCRIPTIONLight grey yellowish medium grained sandstone
BSEN 12407: 2000
APPARENT DENSITY 2427 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 8.7% BSEN 1936: 2006
FLEXURAL STRENGTH (PARALLEL) MEANFLEXURAL STRENGTH (PERPENDICULAR) MEAN
7.3 MPa10 MPa BSEN 13161: 2008
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
Moselden is a popular Yorkstone that has been used on some of the mostprestigious projects in the UK. Its buff appearance contains subtle crescent shaped veining running throughout the stone.
A Carboniferous sandstone from
the Moselden Quarry in West
Yorkshire. Moselden is a very durable
sandstone chosen for a wide variety of
projects nationwide.
West Yorkshire
British Yorkstone MOSELDEN
British Yorkstone MOSELDEN
1817
PHYSICAL PERFORMANCE OF HASLINGDEN BED
GEOLOGICAL TYPEMillstone Grit Series, CarboniferousSandstone
PETROGRAPHIC DESCRIPTION Pale greenish grey fine grained sandstone BSEN 12407: 2000
APPARENT DENSITY 2551 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 5% BSEN 1936: 2006
FLEXURAL STRENGTH (PARALLEL) MEANFLEXURAL STRENGTH (PERPENDICULAR) MEAN
6.1 MPa23.5 MPa BSEN 13161: 2008
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
Haslingden Bed is one of the most popular UK Yorkstones, with a world-class back catalogue of usage. Haslingden Bed possesses extremely high strength making it ideal for a wide variety of usage.
A Carboniferous sandstone from
Lancashire is one of the most popular
sandstones chosen for a wide variety of
projects nationwide.
Lancashire
British Yorkstone HASLINGDEN BED
British Yorkstone HASLINGDEN BED
2019
PHYSICAL PERFORMANCE OF STANTON MOOR
GEOLOGICAL TYPEMillstone Grit Series, CarboniferousSandstone
PETROGRAPHIC DESCRIPTIONBuff to dark buff, fine to medium grained sandstone
BSEN 12407: 2000
APPARENT DENSITY 2290 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 13.3% BSEN 1936: 2006
FLEXURAL STRENGTH (PARALLEL) MEANFLEXURAL STRENGTH (PERPENDICULAR) MEAN
6.7 MPa9 MPa BSEN 13161: 2008
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
A beautiful Derbyshire Carboniferous sandstone that has been used widely across the UK. From major prestigious city centre schemes, to residential developments and private homes, Stanton Moor is a warm buff colour, ideal for all manner of different projects.
A Carboniferous sandstone from the
Dale View Quarry near Matlock Derbyshire. Stanton Moor is one of the most popular sandstones chosen for a wide variety of
projects nationwide.
Matlock, Derbyshire
British Yorkstone STANTON MOOR
British Yorkstone STANTON MOOR
2221
PHYSICAL PERFORMANCE OF ST BEES
GEOLOGICAL TYPE Permo TriassicSandstone
PETROGRAPHIC DESCRIPTION
Dark red to orange/red when wet, fine to medium grained sandstone
BSEN 12407: 2000
APPARENT DENSITY 2140 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 19.8% BSEN 1936: 2006
FLEXURAL STRENGTH (PARALLEL) MEANFLEXURAL STRENGTH (PERPENDICULAR) MEAN
6.3 MPa8.8 MPa BSEN 13161: 2008
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
St Bees is a red sandstone of Permo Triassic age, forming the sea cliffs of St Bees Head near Whitehaven in Cumbria. It is an extremely durable stone, and versatile for all manner of projects.
A Triassic sandstone from the St Bee’s Quarry
in Cumbria, St Bees is a very popular sandstone. Durability and versatility
means it is chosen for a wide variety of
projects as far as the United States.
Cumbria
British Sandstone ST BEES
British Sandstone ST BEES
2423
PHYSICAL PERFORMANCE OF STOKE HALL
GEOLOGICAL TYPEMillstone Grit Series, CarboniferousSandstone
PETROGRAPHIC DESCRIPTIONModerately sorted well compacted Sub Arkose sandstone
BSEN 12407: 2000
APPARENT DENSITY 2350 Kgm -3 BSEN 1936: 2006
OPEN POROSITY 11.1% BSEN 1936: 2006
FLEXURAL STRENGTH (PARALLEL) MEANFLEXURAL STRENGTH (PERPENDICULAR) MEAN
5.4 MPa7.4 MPa BSEN 13161: 2008
This data is an indication of the future performance of the natural stone product only. Full testing and European Conformity marking (CE marking) is the responsibility of the contractor and/or stone processor selling the finished product. Marshalls accepts no liability for any reliance on information/images provided herein or for any contractor and/or stone processor failing to carry out its own testing and inspection.
Test results may not be representative of the entire quarry. The information given is for guidance only and is subject to alteration without notice. Stone is a natural product which is subject to natural formation characteristics, significant variations in colour, texture and technical properties within the same range of stone. The stone image on this page is only as accurate as reprographic processes allow. Marshalls makes no representation or guarantee that the colour or texture shown in print is the same as that of the products delivered.
A fine to medium grained buff sandstone from the Carboniferous period, this versatile stone has been extracted from Stoke Hall quarry at Grindleford since 1835. Stoke Hall has a superb heritage with a number of significant commercial and civic buildings using the stone to great effect.
A Carboniferous sandstone from the Stoke Hall Quarry in
Derbyshire. Stoke Hall is popular because of its even buff colouration
and works well for a variety of projects.
Derbyshire
British Sandstone STOKE HALL
British Sandstone STOKE HALL
2625
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